4. Structure/ Composition of Earth Flashcards

1
Q

What is Mantle convection?

A
  • process that recycles basalt
  • created at spreading ridges, passed along oceanic crust until subducted again
  • whole- mantle versus layered- mantle
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2
Q

What is decompression melting/ Adriatic rise?

A
  • When convection currents bring mantle rock up beneath the spreading ridge
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3
Q

What is incongruent melting?

A
  • when a rock doesn’t melt uniformly.

- Partially melting a rock means the melt has a different composition from the bulk rock

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4
Q

Talk about incongruent melting in the context of the Earth’s mantle?

A
  • basalt is a partial extract of the mantle, leaving behind peridotite
  • peridotite + basalt = rock that basalt is made of
  • could be garnet- peridotite / Lherzolite or pyrolite (has peridotite and basalt)
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5
Q

What is whole-mantle convection versus layered mantle convection?

A
  • whole mantle: convection currents carrying heat from the interior to the planet’s surface
  • layered-mantle- convection currents occur at lower and upper mantle
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6
Q

What is the transition zone?

A
  • between upper and lower mantle where seismic waves change velocity because of different composition
  • where minerals absorb huge amount of water in crystal structures
  • 410-660 km
  • high temperature and pressures compress olivine to wadsleyite; deeper down, wadsleyite–> ringwoodite–> bridgmanite and ferropericlase
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7
Q

Tell the km of upper mantle, transition zone, lower mantle, Core-mantle boundary.

A

0-410- upper mantle
410-660 transition zone
660- 2900 lower mantle
2900 core-mantle boundary

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8
Q

Who was Richard Oldham? Who was Inge Lehmann?

A
  • Richard Oldman: British seismologist who discovered the core. 1906
  • Inge Lehmann: Danish seismologist who discovered liquid outer core
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9
Q

What is the geodynamo?

A
  • Earth’s magnetic field

- has directionality- a positive and negative end that may be steered by convection currents.

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10
Q

What is the most common rock on Earth’s surface?

A

Basalt. Because it forms oceanic crust, which covers 75% of Earth’s surface

  • generated at spreading ridges
  • recycled through mantle convection
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11
Q

Do we know if it’s whole-mantle versus layered-mantle convection?

A

Nope. We don’t know the answer.

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12
Q

What is the Earth’s core largely made of? Are there oxides in crust?

A
  • metallic iron and iron-nickel alloy

- no metallic iron in crust because there’s too much oxygen, which turns iron into different oxides

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13
Q

What is the lower mantle made of?

A

Silciate materials

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14
Q

How fast do seismic waves travel?

A

Few thousand meters/ second

7000 miles/ hour

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15
Q

How do we know the outer core is liquid?

A
  • We know P-waves travel through liquid, but S-waves don’t because liquid isn’t shear enough
  • When an earthquake happens, we see P-waves, but don’t see S-waves on opposite side of earth. Absence of S waves mean outer core is molten
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16
Q

Tell me about earth’s magnetic field.

A
  • generated at liquid outer core
  • protects Earth from solar wind-supercharged particles from sun that would cause UV radiation, damage ozone.
  • direction changes every hundred thousand years. Last was 800,000 yrs ago.
  • direction recorded by ocean crust
17
Q

When was the last time the magnetic field changed direction? How do we know?

A
  • 800,000 years ago magnetic field flipped

- the direction was recorded by the ridge’s ocean crust

18
Q

What is the structure of the inner core?

A
  • inner core behaves like giant crystal
  • iron is HCP- hexagonal-closed packed
  • Iron is anisotropic- meaning seismic waves pass through one direction of crystal faster than the other. Seismic waves pass through inner core faster top down than side by side
19
Q

What structure is iron at inner core versus room temp/pressure?

A

Hexagonal closed packed at core

Room pressure/ temperature- iron is body- centered cubic

20
Q

What is anisotropic?

A

Waves pass through one direction faster than the other.

- Inner core of Earth, iron is hexagonal-closed packed. Seismic waves pass faster top down rather than side by side.